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Introduction and History


Kinabalu Park was established in 1964 and covers an area of 750 square kilometers (300 square miles).  Two expeditions to explore the mountain and its flora in 1961 and 1964 were led by Professor John Corner, on behalf of the Royal Society of London, which led to the formation of Kinabalu Park.


The Park is situated in the East Malaysian state of Sabah (British North Borneo before 1963) and stretches through the entire west coast of Sabah.  Its highest peak is Mount Kinabalu standing at 4101 meters (13,455 feet) visible from the South China Sea.  Being the world’s youngest granite pluton, it continues to rise 5mm/year.


The lowest elevation in Kinabalu Park is at Poring Hot Springs (550 meters/1,805 feet), which lies near the Park’s southern boundary. Therefore temperatures decrease from 25 C hot and humid at Poring to a cool and crisp 4C at Mount Kinabalu’s summit. The climatic changes provide a diverse range of habitats for thousands of plant species.


Due to the high altitude, clouds are trapped in many parts of the Park and heavy rainfall occurs for several months of the year from October to January while February to May are generally the driest months. A common climatic feature of the Park, are bright early mornings, followed by clouds mid-morning which obscure the mountains by mid-day.








Mount Kinabalu is the tallest Malaysian mountain. The next two highest peaks being Mount Trus Madi (8,666 feet) and Mount Tambuyukon (8,462 feet) located 50 kilometers south and 20 kilometers north of Mt Kinabalu respectively. A total of six unique major topographical features occur with Kinabalu Park. These include peaks and plateaus, gullies, rivers, streams and waterfalls, hot springs, caves (Paka Caves and the tumbled bats cave at Poring) and granite slabs, a characteristic of the slopes of the summit.




Mount Kinabalu comprises an oval-shaped granite dome which resulted 1.5 million years ago by volcanic, tectonic and geological processes. Rapid uplift followed by glacial erosion during the Ice Age contributed to the smooth rock surface, which is well graded and paved at the summit. Low's Gully is the most spectacular feature of the mountain spliting it into two peak forming the Western and Eastern Summit Plateau.





Kinabalu Park has essentially four main vegetation zones.  However, these zones are localized variations depending on factors such as soil type, terrain, presence or absence of soils, proximity to streams and degree of exposure to sunlight.  At altitudes above 1200 meters (4,000 feet) it is a place for plants of Himalayan and Chinese genera and for plants of Australian and New Zealand and even American affinity which consist of, among others, buttercups (of Australian affinity), the Rosaceous trees and shrubs and Violets (both of which are of Sino-Himalayan affinity) and they mingle with pitcher plants (Nepenthes) and bamboos of Bornean origins.





A recent study by Beaman & Beaman (1998) found that Kinabalu contains as many as 5,000 to 6,000 species, comprising of over 200 families. More than half (78 species) of the 135 species of Ficus can be found at the site making Mount Kinabalu one of the richest and most diverse assemblages of plants in the world.


There are believed to be 1,000 orchid species, including at least five species of slipper orchid, of the genus Papiopedillium, perhaps the most famous orchid species found on Kinabalu, but they are rarely seen due to intensive collecting for commercial use. Other magnificent orchids are mainly Eria, Bulbophyllum, Dendrobium, Liparis, Dendrochilum, Pholidota, and Coelogyne.


Over 600 fern species are found within the Park, comprising of tree ferns, shade ferns, thicket ferns, epiphytic ferns and tiny scrub ferns.  Nest ferns (Asplenium nidus) are found on every walk at the Park. 


One of the rarest plants in the world – the Rafflesia is only found in very few locations in Borneo.  Named after Sir Stamford Raffles (who founded Singapore in 1819), it is the largest flower in the world.  Two species, R. Keithii and R. Pricei have been found in the Park in the Poring Hot Springs area.  In recent years, a third species, R. Tengku-Adlini was discovered.



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